254 
LAMPLUGH : GLACIAL SECTIONS. 
Might one expect to find traces of Kryokonite in any of our 
glacial clays ? 
In the first part of this paper I stated my views on the subject 
of the intermingling of these gravels with the Purple Boulder Clay ; 
in the second part, on the origin of the stratified band and interca- 
lary sand and gravel in the Purple Clay ; in the Geological Magazine^ 
for September, 1879, I have described the Laminated Clay ; in the 
same magazine for December, 1881, and possibly also in a forthcom- 
ing number of the Quart. Jour. Geol. Soc, I have dealt with the 
Basement Boulder Clay and its included fragments of beds ; and 
with the present paper it is probable that this series will close. Not 
from want of matter, for there are problems enough in this, as in 
most neighbourhoods, to suffice for many lives, but from the current 
of events which will separate me from my work. 
I have to thank Messrs. Dobb & Gummer, the contractors for 
the drainage works, for the facilities and information they have so 
courteously rendered me during the course of the work ; and J. S. 
Moloney, Esq., C.E., for his kind advice and aid in preparing the 
plan and sections. 
ON THE SHELL MOUNDS OR KITCHEN MIDDENS AT SPURN POINT. 
BY H. BENDELAK HEWETSON. 
(Publication deferred.) 
THE YOUNG STAGE OF SOME CARBONIFEROUS CEPHALOPODA 
BY WM. CASH, F.G.S. 
(Publication deferred.) 
